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Seasonal Performance of a Nonhydrostatic Global Atmospheric Model on a Cubed-Sphere Grid

Title
Seasonal Performance of a Nonhydrostatic Global Atmospheric Model on a Cubed-Sphere Grid
Authors
Kim J.-E.E.Koo M.-S.Yoo C.Hong S.-Y.
Ewha Authors
유창현
SCOPUS Author ID
유창현scopus
Issue Date
2021
Journal Title
Earth and Space Science
ISSN
2333-5084JCR Link
Citation
Earth and Space Science vol. 8, no. 4
Keywords
GCMGRIMsKIMmodel comparisonseasonal predictionweather forecast
Publisher
Blackwell Publishing Ltd
Indexed
SCIE; SCOPUS WOS scopus
Document Type
Article
Abstract
The Korean Integrated Model (KIM), a recently developed nonhydrostatic global atmospheric model over a cubed-sphere grid, was deployed in April 2020 as an operational weather forecasting model. As its application extends to research and predictions longer than the weather time scale, we evaluated the ability of the KIM on seasonal ensemble simulation for the boreal winter and summer cases with respect to seasonal mean biases. The results are compared with those obtained from a conventional hydrostatic spectral model, which has been widely used for seasonal simulations and in climate research. To isolate the origin of the error sources, the same physics packages is used in both the KIM and the reference models. The simulated mean states are very close to the reanalysis for the selected cases. Most large-scale fields from the KIM are comparable to those from the reference model, which implies that the general features of large-scale variables and precipitation are highly governed by physical parameterizations, and that the physics-dynamics coupling is stable in a long-term simulation. Large-scale tropical circulations, such as the Hadley and Walker circulations, need to be improved for applications related to future changes and climate projections. Moreover, the results reveal that the simulated global precipitation band is misplaced and the heat fluxes over oceans are relatively misrepresented near the eastern boundaries of tropical and subtropical regions. This analysis suggests the necessity of realistic atmosphere-ocean interactions that reflect ocean overturning circulation via ocean coupling as well as the refinement of deep and shallow convection schemes. © 2021. The Authors. Earth and Space Science published by Wiley Periodicals LLC on behalf of American Geophysical Union.
DOI
10.1029/2021EA001643
Appears in Collections:
공과대학 > 기후에너지시스템공학과 > Journal papers
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